ERCOFTAC Series
DOI: 10.1007/978-1-4020-6218-6_21
|View full text |Cite
|
Sign up to set email alerts
|

Lagrangian multi-particle statistics

Abstract: Combined measurements of the Lagrangian evolution of particle constellations and the coarse grained velocity derivative tensor ∂ ui/∂xj are presented. The data is obtained from three dimensional particle tracking measurements in a quasi isotropic turbulent flow at intermediate Reynolds number. Particle constellations are followed for as long as one integral time and for several Batchelor times. We suggest a method to obtain quantitatively accurate ∂ ui/∂xj from velocity measurements at discrete points. We obta… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

1
23
1

Publication Types

Select...
6
2

Relationship

0
8

Authors

Journals

citations
Cited by 18 publications
(25 citation statements)
references
References 27 publications
1
23
1
Order By: Relevance
“…The orthogonality betweenẽ ω and e 3 also decreases with increasing scale. These results are consistent with previous data (Luthi et al 2007;Pumir et al 2013;Danish & Meneveau 2018) whereà was computed using different coarse-graining methods. In figure 5(b), we see that vorticity reaches a peak alignment with e R1 after a time delay of t ≈ 3τ N , almost independent of the scale l/η (Xu et al 2011;Pumir et al 2013).…”
Section: Vorticity Alignmentsupporting
confidence: 93%
“…The orthogonality betweenẽ ω and e 3 also decreases with increasing scale. These results are consistent with previous data (Luthi et al 2007;Pumir et al 2013;Danish & Meneveau 2018) whereà was computed using different coarse-graining methods. In figure 5(b), we see that vorticity reaches a peak alignment with e R1 after a time delay of t ≈ 3τ N , almost independent of the scale l/η (Xu et al 2011;Pumir et al 2013).…”
Section: Vorticity Alignmentsupporting
confidence: 93%
“…6 and 7 is that it is not possible to either identify a clear Richardson scaling or distinguish between Richardson and Batchelor scaling from these figures. This limitation is quite common to numerical studies based on direct numerical simulation 16,55 but was also encountered in experiments, 56,57 and arises because the flow Reynolds number is not large enough to provide the separation of scales that is required to observe a wide enough inertial range. It is thus believed that a broad crossover from the dissipation regime (in which separation grows exponentially) to the diffusion regime exists that hides the intermediate inertial range regime.…”
Section: (T)mentioning
confidence: 99%
“…The velocity gradients constitute a convenient descriptor of the fundamental structure of turbulent flows and some of their statistics reflect the out-of-equilibrium nature of turbulence. Although the velocity gradients describe only the structure of the small scales, the statistical distributions of the filtered velocity gradients are invariant across scales and reveal the self-similar structure of the inertial range [30,80,107,108]. Some investigations suggest a connection between the velocity gradients in the inertial scales and the energy cascade [30,40,109], and common SGS models rely on the assumption that energy transfer towards the unresolved scales can be reproduced using the velocity gradients of the resolved scales [85,97,110].…”
Section: Direct Cascadesmentioning
confidence: 99%